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Bi 2Te 1.6S 1.4: A topological insulator in the tetradymite family

Author(s): Ji, Huiwen; Allred, Jared M.; Fuccillo, Michael K.; Charles, M.E.; Neupane, Madhab; et al

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dc.contributor.authorJi, Huiwen-
dc.contributor.authorAllred, Jared M.-
dc.contributor.authorFuccillo, Michael K.-
dc.contributor.authorCharles, M.E.-
dc.contributor.authorNeupane, Madhab-
dc.contributor.authorWray, Lewis Andrew-
dc.contributor.authorHasan, M. Zahid-
dc.contributor.authorCava, Robert Joseph-
dc.date.accessioned2019-08-29T17:06:02Z-
dc.date.available2019-08-29T17:06:02Z-
dc.date.issued2012-05en_US
dc.identifier.citationJi, Huiwen, Allred, J.M., Fuccillo, M.K., Charles, M.E., Neupane, M., Wray, L.A., Hasan, M.Z., Cava, R.J. (2012). Bi Te S : A topological insulator in the tetradymite family. Physical Review B, 85 (20), 10.1103/PhysRevB.85.201103en_US
dc.identifier.issn1098-0121-
dc.identifier.urihttp://arks.princeton.edu/ark:/88435/pr13156-
dc.descriptionPhysical Review B - Condensed Matter and Materials Physics. Volume 85, Issue 20, 15 May 2012, Article number 201103.en_US
dc.description.abstractWe describe the crystal growth, crystal structure, and basic electrical properties of Bi 2Te 1.6S 1.4, which incorporates both S and Te in its tetradymite quintuple layers in the motif -[Te 0.8S 0.2]-Bi-S-Bi-[Te 0.8S 0.2]-. This material differs from other tetradymites studied as topological insulators due to the increased ionic character that arises from its significant S content. Bi 2Te 1.6S 1.4 forms high quality crystals from the melt and is the S-rich limit of the ternary Bi-Te-S γ-tetradymite phase at the melting point. The native material is n type with a low resistivity; Sb substitution, and with adjustment of the Te to S ratio, results in a crossover to p type and resistive behavior at low temperatures. An angle-resolved photoemission study shows that topological surface states are present, with the Dirac point more exposed than it is in Bi 2Te 3 and similar to that seen in Bi 2Te 2Se. Single crystal structure determination indicates that the S in the outer chalcogen layers is closer to the Bi than the Te, and therefore that the layers supporting the surface states are corrugated on the atomic scale. © 2012 American Physical Society.en_US
dc.format.extent85.20:201103-1 - 201103-5en_US
dc.language.isoen_USen_US
dc.relation.ispartofPhysical Review Ben_US
dc.rightsFinal published version. This is an open access article.en_US
dc.titleBi 2Te 1.6S 1.4: A topological insulator in the tetradymite familyen_US
dc.typeJournal Articleen_US
dc.identifier.doidoi:10.1103/PhysRevB.85.201103-
dc.date.eissued2012-05-15en_US
dc.identifier.eissn1550-235X-
pu.type.symplectichttp://www.symplectic.co.uk/publications/atom-terms/1.0/journal-articleen_US

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